{"id":156184,"date":"2026-01-12T17:26:54","date_gmt":"2026-01-12T17:26:54","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/fluidos-mineralizadores-en-los-yacimientos-de-oro-de-saucelle-y-el-cabaco-salamanca\/"},"modified":"2026-01-12T17:26:54","modified_gmt":"2026-01-12T17:26:54","slug":"fluidos-mineralizadores-en-los-yacimientos-de-oro-de-saucelle-y-el-cabaco-salamanca","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/fluidos-mineralizadores-en-los-yacimientos-de-oro-de-saucelle-y-el-cabaco-salamanca\/","title":{"rendered":"Fluidos mineralizadores en los yacimientos de oro de saucelle y el cabaco (salamanca)"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Antona Blazquez J. Francisco <\/strong><\/h2>\n<p>Se han estudiado las caracteristicas de los fluidos mineralizadores en los yacimientos filonianos de oro de saucelle y de el cabaco (salamanca); para ello se ha realizado un detallado estudio de campo de estos filones y un trabajo de laboratorio que ha consistido en: * estudios petrograficos.  * Estudios microtermometricos de inclusiones fluidas en cuarzo.  * Separacion de minerales: arsenopirita, pirita, moscovita y cuarzo.  * difraccion de rayos x.  * Y analisis geoquimicos (elementos mayores y trazas, analisis puntual con microsonda electronica, analisis de isotopos estables de s, o, h y dataciones k\/ar en moscovitas). Finalmente, se concluye que los fluidos en estos yacimientos tienen un origen metamorfico y el oro fue transportado en condiciones reductoras y moderadamente acidas, precipitando como consecuencia de la inmiscibilidad de un fluido original. Se constata, asimismo, la mayor concentracion de oro en los filones proximos a los contactos de los granitos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Fluidos mineralizadores en los yacimientos de oro de saucelle y el cabaco (salamanca)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Fluidos mineralizadores en los yacimientos de oro de saucelle y el cabaco (salamanca) <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Antona Blazquez J. Francisco <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1991<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Antonio Garcia Sanchez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Emilio Galan Huertas <\/li>\n<li>Antonio Gutierrez Maroto (vocal)<\/li>\n<li>E. Fallick Anthony (vocal)<\/li>\n<li>Jos\u00e9 Navarrete Lopez-cozar (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Antona Blazquez J. Francisco Se han estudiado las caracteristicas de los fluidos mineralizadores en los yacimientos filonianos [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,953,9386,3612],"tags":[270288,40935,39466,270290,270289,270291],"class_list":["post-156184","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-salamanca","category-yacimientos-minerales","tag-antona-blazquez-j-francisco","tag-antonio-garcia-sanchez","tag-antonio-gutierrez-maroto","tag-e-fallick-anthony","tag-emilio-galan-huertas","tag-jose-navarrete-lopez-cozar"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/156184","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=156184"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/156184\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=156184"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=156184"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=156184"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}